CCD卫星相机时间序列定标:以CBERS02B为例     

高海亮  顾行发  余涛  李小英  巩慧  李家国 《测绘学报》2011,40(2):180-187

采用沙漠场景法、稳定目标法和交叉定标法对CBERS02B星的CCD相机开展时间序列定标,分别得到CCD相机2007-2008年期间三种方法对应的定标系数,并同CBERS02B卫星官方提供的定标系数进行比对.结果表明,三种方法得到的定标系数其误差均小于10%,不同方法的结果具有较好的一致性.最后,分析总结各种时间序列定标...  相似文献   

A robust potential-based contact force solution approach for discontinuous deformation analysis of irregular convex polygonal block/particle systems     

Zheng  Fei  Zhuang  Xiaoying  Zheng  Hong  Jiao  Yu-Yong  Rabczuk  Timon 《Acta Geotechnica》2021,16(3):679-697

Acta Geotechnica - Contact interaction of two bodies can be modeled using the penalty function approach while its accuracy and robustness are directly associated with the geometry of contact...  相似文献   

Petrological and zircon evidence for the Early Cretaceous granulite-facies metamorphism in the Dabie orogen, China     

GAO Xiaoying 《《地质学报》英文版》2018,92(Z2):10-10

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基于弹性地基梁理论的冻胀作用下管道应力分析   总被引：3，自引：1，他引：2  

黄龙  盛煜  胡晓莹  王生廷  黄旭斌  何彬彬 《冰川冻土》2018,40(1):70-78

穿越冻土区的埋地管线在遭遇冻土差异性冻胀时,管道会发生翘曲变形,管线将面临很大的安全隐患。为此,基于弹性地基梁理论建立冻胀条件下的管-土相互作用模型,分析了管道在冻胀及其影响因素作用下的应力分布规律,探讨了冻土地基特性（弹性模量、泊松比及地基系数）与温度的关系,对比了不同地基系数、冻胀量、管径、壁厚、温差以及上覆土厚度等特定条件下的管道应力峰值状况。计算结果表明：管道在过渡段与冻胀段及非冻胀段交界处有最大应力值,各类影响因素对管道交界处的应力影响最显著;地基系数的值越大,差异性冻胀量越大,管径越大,温差越大,管道交界处应力峰值也越大;管壁越厚,在管道交界处的应力峰值越小;管道上覆土层越厚,管道受冻胀作用弯曲应力越小,即加深上覆土层可降低管道由于冻胀抬升所产生的应力,可减缓管道变形。  相似文献   

In-situ experimental research on water scouring of loess slopes     

Xiaoying Qiao  Xi’an Li  Yiwei Guo  Shaoyang Ma 《Environmental Earth Sciences》2018,77(11):417

Frequent occurrence of landslides in the Chinese Loess Plateau has been influenced by the changes of water conditions. This paper, based on in-situ water scouring experiments under various slope gradients, cross-sectional discharge shapes and flow quantities, analyzed the rill flow information characteristics on a loess slope and its driving factors for anti-scourability of the loess stratum. The results show that the critical erosion slope gradient for the loess stratum (Q₃) is about 24° and the mean erosion rate under half-round cross-sectional discharge is smaller than that under rectangular discharge. The relationship between flow quantity and mean erosion rate is linear and is positively correlated. Mechanical subsurface erosion was the primary condition responsible for water scouring on loess slopes because of stronger runoff channels such as vertical joints and large amounts of macro void caused by plants and animals. Loess anti-scourability is a significant issue to advance the research for soil and water conservation in the Loess Plateau of China.  相似文献   

Spatio-temporal variability in remotely sensed surface soil moisture and its relationship with precipitation and evapotranspiration during the growing season in the Loess Plateau,China   总被引：2，自引：2，他引：0  

Xiaoying Li  Lichen Liu  Zhenghu Duan  Na Wang 《Environmental Earth Sciences》2014,71(4):1809-1820

The distribution and variability of surface soil moisture at regional scales is still poorly understood in the Loess Plateau of China. Spatial and temporal dynamics of surface soil moisture is important due to its impact on vegetation growth and its potential feedback to atmospheric and hydrologic processes. In this study, we analyzed surface soil moisture dynamics and the impacts of precipitation and evapotranspiration on surface soil moisture using remote sensing data during the growing season in 2011 for the Loess Plateau, which contain surface soil moisture, precipitation, vegetation index and evapotranspiration. Results indicate that the areas with low surface soil moisture are mainly located in the semi-arid region. Under dry surface soil moisture, evapotranspiration temporal persistence has a higher positive correlation (0.537) with surface soil moisture temporal persistence, and evapotranspiration is very sensitive to surface soil moisture. But under wet surface soil moisture regime, surface soil moisture temporal persistence has a higher negative correlation (?0.621) with evapotranspiration temporal persistence. Correlation of surface soil moisture and monthly precipitation, evapotranspiration and vegetation index illustrated that precipitation was a significant factor influencing surface soil moisture spatial variance. The correlation coefficients between monthly surface soil moisture and precipitation was varied in different climatic regions, which was 0.304 in arid, 0.364 in semi-arid, 0.490 in transitional and 0.300 in semi-humid regions. Surface soil moisture is more sensitive to precipitation, evapotranspiration, in transitional regions between dry and wet climates.  相似文献   

从“路径创造”到“路径锁定”：港澳台投资与外商投资影响珠三角产业动态的比较分析     

钱肖颖  杨宇 《地理科学进展》2022,41(9):1635-1646

随着改革开放的深入,港澳台及外商投资在珠三角地区产业转型过程中的弊端逐渐暴露,部分港澳台/外资企业成为区域发展新路径的阻碍,但已有研究对此讨论不足。因此,论文基于2000—2019年珠三角地区地级市行政区制造业的面板数据,构建了路径依赖与路径突破指数,通过固定面板回归模型,探究比较港澳台投资与外商投资对珠三角地区产业动态的影响。结果发现：港澳台投资有利于路径依赖型新产业出现,促进地方产业的相关多样化发展,更强的本地嵌入性是主要原因;外商投资则会降低地方产业路径突破的可能,并通过强化产业集中度,导致路径锁定。此外,政府补贴会强化外商投资的路径锁定效应。研究结论对完善产业演化理论和优化中国港澳台及外商投资政策导向具有重要启示。  相似文献   

Understanding hydrological trends by combining the Budyko hypothesis and a stochastic soil moisture model     

Zhentao Cong  Xiaoying Zhang  Dan Li  Hanbo Yang  Dawen Yang 《水文科学杂志》2013,58(1):145-155

Abstract

The actual evapotranspiration and runoff trends of five major basins in China from 1956 to 2000 are investigated by combining the Budyko hypothesis and a stochastic soil moisture model. Based on the equations of Choudhury and Porporato, the actual evapotranspiration trends and the runoff trends are attributed to changes in precipitation, potential evapotranspiration, rainfall depth and water storage capacity which depends on the soil water holding capacity and the root depth. It was found that the rainfall depth increased significantly in China during the past 50 years, especially in southern basins. Contributions from changes in the water storage capacity were significant in basins where land surface characteristics have changed substantially due to human activities. It was also observed that the actual evapotranspiration trends are more sensitive to precipitation trends in water-limited basins, but more sensitive to potential evapotranspiration trends in energy-limited basins.